Climate Model Summary

Model Summary forecasts are no longer available

We are streamlining some climate pages including removal of the Model Summary.

From 10 December our climate information is available on the Southern Hemisphere monitoring and Southern Hemisphere outlooks pages.
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Average of international model outlooks for the Niño3.4 index

Average of international model outlooks for the Indian Ocean Dipole (IOD) index

Based on the ensemble mean for the most recent model run.
Dial details

The arrows on the dials indicate the combined average of monthly outlooks from a survey of international global climate models. Note that the individual model runs vary around the average.

The ENSO and IOD dials are calculated by simply averaging the ensemble means from all the models surveyed. Values are not representative of the potential spread of the forecast outcomes. Therefore, the dials are intended to be used as a quick reference to determine whether the models are showing a warming trend, a cooling trend, or neither. More information is provided in the graphs presented in other sections.


 

Niño3.4 covers the central Pacific region.

Niño3.4 multi-model forecast for the months ahead

Graphs

Niño3.4 2 month outlook Models information
Bar graph details

The graphs are based on the ensemble mean for the most recent model run.

These graphs show the average forecast value of Niño3.4 for each international model surveyed for the selected calendar month. If the bars on the graph are approaching or exceeding the blue dashed line, there is an increased risk of La Niña. Similarly, if the bars on the graph are approaching or exceeding the red dashed line, there is an increased chance of El Niño.


 

IOD index multi-model forecast for the months ahead

Graphs

Latest IOD outlook Models information
Bar graph details

The graphs are based on the ensemble mean for the most recent model run.

These graphs show the average forecast value of the IOD index for each international model surveyed for the selected calendar month. If the majority of models are approaching or exceeding the blue dashed line, then there is an increased risk of a negative IOD event. If the majority of models are approaching or exceeding the red dashed line, then there is an increased risk of a positive IOD event.


More information:

Sea surface temperature graphs

Australian climate is influenced by sea surface temperature and atmospheric patterns in the Pacific, Indian and Southern ocean regions. Specific regions are monitored, as they can indicate the presence, or potential development, of ENSO (El Niño/La Niña), Indian Ocean Dipole (IOD) phases and Southern Annular Modes. Pacific and Indian ocean indices are updated fortnightly, but the SAM index can change rapidly so it is updated daily. The first SAM button matches the Niño and IOD fortnightly issue date. During the following fortnight the 'Latest SAM' chart will diverge.

Niño34 predictions for the next 5 months

Long-range forecast graph for selected SST region

Niño34 probabilities

Product code: IDCK000073

Model details

Model selection

All the models included in this page have been documented in the peer-reviewed international scientific literature and have skill in predicting El Niño-Southern Oscillation (ENSO) and Indian Ocean patterns. They are all coupled General Circulation Models, and hence simulate both atmospheric and oceanic processes using physics rather than statistics. Most have been run routinely for a number of years and are subject to regular revision and update with the aim of continuous improvement. They represent the state-of-the-art of climate prediction systems and offer useful guidance up to about nine months. The majority of models used in our survey are formally recognised by the World Meteorological Organization as Global Producing Centres for long-range forecasts.

All models use an ensemble method, where several forecasts are run at the same time using slightly different initial conditions. While all models use ensemble techniques, the number of ensembles differs for each model.

The data presented on these pages is the 'ensemble mean' which is the average of all the model-runs performed by each model, each month. The ensemble mean therefore flattens out the potential forecast outcomes and doesn't show the full spread of the possible forecast scenarios.

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The webpage

This webpage surveys the latest output from several reputable climate models developed at leading international climate agencies. Data from these models is analysed and displayed in graphs and dials to show how temperature patterns in the Indian and Pacific ocean are likely to change over the coming six-months. These patterns in the oceans have been shown to have a significant impact on Australian temperature and rainfall patterns (e.g. cooling of the tropical Pacific Ocean during La Niña events is typically associated with increased rainfall and cooler daytime temperatures in Australia).

When the models are in agreement, then there is higher confidence in the model outlooks. When the models are showing a large spread or large variety of outcomes, there is a larger amount of uncertainty associated with the forecast.

The models

All the models included in this page have been documented in the peer-reviewed international scientific literature and have skill in predicting El Niño-Southern Oscillation (ENSO) and Indian Ocean patterns. They are all coupled General Circulation Models, and hence simulate both atmospheric and oceanic processes using physics rather than statistics. Most have been run routinely for a number of years and are subject to regular revision and update with the aim of continuous improvement. They represent the state-of-the-art of climate prediction systems and offer useful guidance up to about nine months. The majority of models used in our survey are formally recognised by the World Meteorological Organization as Global Producing Centres for long-range forecasts.

Update schedule

The Climate Model Summary is updated on the 12th of each month (or the next working day following the 12th) when model data becomes available. Data for the Bureau's model, ACCESS–S, is updated fortnightly along with several other models that also provide more frequent updates during the month.

The ensemble technique

All models use an ensemble method, where several forecasts are run at the same time using slightly different initial conditions. While all models use ensemble techniques, the number of ensembles differs for each model.

Important note

The data presented on these pages is the 'ensemble mean' which is the average of all the model-runs performed by each model, each month. The ensemble mean therefore flattens out the potential forecast outcomes and doesn't show the full spread of the possible forecast scenarios.

The dials

The ENSO and IOD dials (from the Overview section) are calculated by simply averaging the ensemble means from all the models surveyed. Values are not representative of the potential spread of the forecast outcomes. Therefore, the dials are intended to be used as a quick reference to determine whether the models are showing a warming trend, a cooling trend, or neither. More information is provided in the graphs presented in other sections.


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Model data are provided for Bureau of Meteorology use by the agencies detailed in Model Summary – Models. Respective agency copyright applies to these data.

Models suggest ENSO neutral through austral autumn

The El Niño-Southern Oscillation (ENSO) is likely to remain neutral throughout the austral autumn with most climate models suggesting sea surface temperatures in the tropical Pacific Ocean will remain near the long-term average until at least May 2017.

While all models indicate a gradual warming of ocean temperatures in the tropical Pacific over the next six months, two models suggest a more rapid warming with El Niño thresholds exceeded by June. The remaining models maintain temperatures consistent with a neutral ENSO throughout the outlook period. It also must be noted that this outlook straddles the autumn predictability barrier - typically the ENSO transition period - during which most models have their lowest forecast accuracy.

NINO3.4 outlook

The latest NINO3.4 outlooks (issued in January) indicate temperatures in the central tropical Pacific, which have been cooler than average since July 2016, are likely to warm gradually over the next six months. However, model consensus suggests the El Niño-Southern Oscillation (ENSO) will remain neutral until at least the end of the southern autumn.

The most recent weekly NINO3.4 value to 15 January is −0.3 °C. By April, the all model average is +0.2 °C suggesting consistent warming over the coming months. By June, two models exceed the El Niño threshold with a third model falling just short. It must be noted that this outlook straddles the autumn predictability barrier - typically the ENSO transition period - during which most models have their lowest forecast accuracy. Thus, outlooks beyond May should be used with caution.

The Bureau routinely monitors oceanic and atmospheric conditions and model outlooks. NINO3.4 values that persist below −0.8 °C typically indicate a La Niña event has become established, while persistent values above +0.8 °C typically indicate El Niño.

Indian Ocean Dipole (IOD) outlook

The latest weekly IOD index value to 15 January is –0.2 °C, continuing within the neutral range. The IOD is typically unable to form between December and April, when the monsoon trough becomes active in the southern hemisphere. It has little impact on Australian climate at this time of year.

The 2016 negative IOD event is considered one of the strongest such events in at least 50 years and had a significant impact on winter and spring rainfall in Australia during 2016. 

Predictive Ocean Atmosphere Model for Australia (POAMA)

POAMA, run at the Bureau of Meteorology, generates an eight-month forecast each fortnight. The most recent model run (generated 1 January) indicates NINO3.4 will remain slightly cooler than average, but within ENSO neutral boundaries, throughout the summer months, warming to near-zero by March 2017.

By mid-winter, POAMA suggests a ~30% chance of temperatures in the NINO3.4 region reaching values consistent with El Niño, however, this forecast straddles the autumn predictability barrier, meaning forecast skill beyond autumn is low. The ensemble mean during the winter months remains just within neutral boundaries.

The forecast values, shown below in bold, are for POAMA's ensemble mean.

Product code: IDCKGL0000

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